ABSTRACT
Introducción: Debido a su extensión actual, la biomasa radicular de los pastizales tropicales es de vital importancia para el almacenamiento del carbono terrestre, pero su estimación ha sido principalmente indirecta y con un rango muy amplio de valores. Objetivo: Documentar a nivel nacional y mundial, y comparar, las existencias de carbono radicular extraídas en forma directa, de dos pastizales de origen y tipo de crecimiento distinto. Método: Se midió la biomasa y carbono total de dos pastizales con más de 40 años de uso, uno nativo de América y de crecimiento estolonífero (Paspalum notatum) y otro introducido de África y de crecimiento en macollos (Urochloa decumbens). El estudio se realizó entre agosto y octubre 2016. Se seleccionaron 3 parcelas de 1 600 m2 por pastizal, con 10 subcuadros (4 m2 c/u) en cada parcela, para determinar composición florística, biomasa y C aéreo. La biomasa y C radicular se estimaron mediante extracción directa en tres trincheras (1.50 m x 0.50 m x 1.0 m) por parcela. El contenido de carbono orgánico se determinó con el método por ignición a una temperatura promedio de 550 °C durante 3 horas. Para el análisis estadístico se usó un ANOVA de dos factores, en el que un factor fueron dos tratamientos (tipo de pastizal) y el otro factor fue la parte morfológica del pasto (aéreo y radicular). Resultados: La composición florística de los dos tipos de pastizal fue diferente debido a su historia de manejo. En promedio se estimó 28.25 MgC ha-1 total para la localidad. El pastizal nativo y de crecimiento estolonífero P. notatum produce casi tres veces más biomasa (42.5 MgC ha-1) que el introducido y de crecimiento en macollos U. decumbens (14 MgC ha-1) debido al almacén radicular (38.5 vs. 11.46 MgC ha-1). El 74.5 % del carbono en P. notatum se localizó en la parte radicular y el 25.5 % en la parte aérea, mientras que en U. decumbens fueron 56.5 y 43.5 %, respectivamente. Conclusión: P. notatum acumuló más biomasa y carbono total y radicular que U. decumbens. La mejor adaptación del pasto nativo, así como la morfología de su sistema radicular, pueden explicar esta diferencia. El 96 % de la biomasa y del C radicular se encuentra en los primeros 0.50 m de profundidad. Debido a la contribución de su porción radicular, los pastizales tropicales pueden constituir importantes reservorios de carbono terrestre, considerando su extensión hoy en día.
Introduction: Due to its current coverage, the root biomass of tropical pastures is of vital importance for the terrestrial carbon storage, but its estimation has been mainly indirect and with a very wide range of values. Objective: To document at national and global level as well as compare, the root carbon stocks extracted directly from two grasslands of different growth type and origin. Methods: The biomass and root carbon stocks were directly extracted from two tropical pastures with more than 40 yr of age. The biomass and total carbon, one native with stoloniferous growth (Paspalum notatum) and one introduced with growth in tillers (Urochloa decumbens) were measured. The study was conducted between August and October 2016. Three plots of 1 600 m2 each were selected per pasture, with 10 sub-squares (4 m2 each) in each plot to determine the floristic composition, aboveground biomass and C. The biomass and root C were estimated by hand in three trenches (1.50 m x 0.50 m x 1.0 m) per plot. The organic carbon content was determined with the ignition method at an average temperature of 550 °C for 3 hours. For the statistical analysis, a two-factor ANOVA was used, where one factor was the treatments that were the type of pasture (2) and the other factor was the section of the grass (above and belowground). Results: The floristic composition of the two types of pasture was different due to its management history. On average, 28.25 Mg ha-1 of total C was estimated for the locality. The native pasture of stoloniferous growth P. notatum yields almost three-fold more biomass (42.5 MgC ha-1) than the introduced with growth in tillers U. decumbens (14 MgC ha-1) due to the radicular storage (38.5 vs. 11.46 MgC ha-1). Seventy-four point five percent of the carbon in P. notatum was located in the radicular part and 25.5 % above-ground, while in U. decumbens 56.5 and 43.5 %, respectively. Conclusions: P. notatum accumulated more total and radicular biomass and carbon than U. decumbens. The best adaptation of the native grass as well as the morphology of its root system may explain this difference. Ninety six percent of the biomass and root C is found in the first 0.50 m depth. Due to the contribution of its radicular portion, tropical pastures can constitute important reservoirs of terrestrial carbon considering its extension nowadays.
ABSTRACT
The last destination of most herbicides used in agricultural systems is the soil. This is a dynamic interaction; herbicides can remain in the soil solution or be carried through the soil profile, reaching the water table. The objective of this work was to evaluate the leaching potential of the tebuthiuron herbicide using bioindicator plants grown in an Oxisol of sandy loam texture and in an Entisol of clay texture, after the occurrence of natural rainfall events. A complete randomized experimental design was used, in a 3×8 factorial arrangement, with four replications. The treatments consisted of three accumulated natural rainfall depths (30-40, 60-80, and 100-120 mm) and eight soil profile layers (0-3, 3-6, 6-9, 9-12, 12-15, 15-20, 20-25, and 25-30 cm). Soil samples were collected after the tebuthiuron herbicide application - 750 for clayey soil, and 600 g ha-1 for the sandy loam soil -and the rainfall events. PVC pipes with length of 30 cm and diameter of 15 cm were introduced into the soil profile for sampling. The pipes with soil columns were carefully removed by digging around them, to maintain the soil original integrity during collection and, subsequently, cut longitudinally for sowing the bioindicator species - cucumber (Cucumis sativus L.), and lettuce (Lactuca sativa L.). Then, the phytotoxicity in the bioindicator plants grown in these soils were evaluated at 5, 7, 10, and 12 days after sowing, using a grading scale of 0 to 100%. The mobility of the tebuthiuron herbicide was low in both soils, regardless of the rainfall depth, and the cucumber was the most suitable plant species to use as a bioindicator.(AU)
O solo é o destino final da maioria dos herbicidas utilizados no sistema agrícola e, sendo esta relação dinâmica, eles podem permanecer na solução ou ser carregados no perfil do solo, podendo atingir o lençol freático. O objetivo deste trabalho foi avaliar o potencial de lixiviação do herbicida tebuthiuron por meio de plantas bioindicadoras e após a ocorrência de precipitações pluviométricas naturais, em solos com texturas franco arenoso (Latossolo Vermelho-Amarelo) e argiloso (Neossolo Litólico). O delineamento experimental foi o inteiramente casualizado em um esquema fatorial 3 x 8 com quatro repetições, sendo três níveis de precipitação pluviométrica (30-40, 60-80 e 100-120 mm) e oito de profundidade do perfil do solo (0-3, 3-6, 6-9, 9-12, 12-15, 15-20, 20-25 e 25-30 cm). As coletas das amostras ocorreram após a aplicação do herbicida tebuthiuron nas doses de 750 e 600 g ha-1 para o solo argiloso e arenoso, respectivamente, e posterior acúmulo das precipitações. Para a coleta das amostras foram introduzidas, no perfil do solo, colunas de PVC com 30 cm de altura e 15 cm de diâmetro. As colunas foram retiradas cuidadosamente escavando-se ao seu redor, mantendo a integridade original do solo durante a coleta. Posteriormente, as colunas foram separadas com corte longitudinal, para a semeadura das espécies bioindicadoras pepino (Cucumis sativus L.) e alface (Lactuca sativa L.). Para as avaliações das plantas bioindicadoras nas colunas, adotou-se a escala de notas de 0 a 100% de fitotoxicidade, aos 5, 7, 10 e 12 dias após a semeadura. A mobilidade do herbicida tebuthiuron mostrou-se reduzida em ambos os tipos de solo estudado, independentemente da precipitação pluvial, e as plantas de pepino mostraram-se mais adequadas para serem utilizadas como espécie bioindicadora.(AU)
Subject(s)
Soil , Percolation , Environmental Biomarkers , Herbicides , Plants , Rain , Plant WeedsABSTRACT
En el presente estudio se realizó una selección de cuatro sitios con alta presencia de poblaciones de chile silvestre en un área de 85 km2, correspondiente al municipio de Mocorito, Sinaloa, México. Mediante la observación en campo, se decidió realizar un perfil de suelo en cada uno de los sitios, el cual consistió en la descripción de campo, análisis físico-químico e hidrofísico y la clasificación de los diferentes tipos de suelo. De esta forma se logró identificar un tipo de suelo por cada población de chile silvestre, estos corresponden al tipo de suelo Vertisol, Fluvisol, Leptosol y Feozem.
A selection of four sites was performed with high presence of populations of wild chilli in an area of 85 km2, corresponding to the municipality of Mocorito, Sinaloa, Mexico. Through field observations, it was decided to conduct a soil profile on each of the sites, which consisted in the description field and hidrofísico physicochemical analysis and classification of differents types of soil. Thus was identified a type of soil per population of wild chilli, these correspond to soil type Vertisol, Fluvisol, Leptosol and Feozem.
Subject(s)
Clay Soils , NatureABSTRACT
Arbuscular mycorrhizal fungi (AMF) colonize land plants in every ecosystem, even extreme conditions such as saline soils. In the present work we report for the first time the mycorrhizal status and the vertical fungal distribution of AMF spores present in the rhizospheric soil samples of four species of Chenopodiaceae (Allenrolfea patagonica, Atriplex argentina, Heterostachys ritteriana and Suaeda divaricata) at five different depths in two saline of central Argentina. Roots showed medium, low or no colonization (0-50%). Nineteen morphologically distinctive AMF species were recovered. The number of AMF spores ranged between 3 and 1162 per 100 g dry soil, and AMF spore number decreased as depth increased at both sites. The highest spore number was recorded in the upper soil depth (0-10 cm) and in S. divaricata. Depending of the host plant, some AMF species sporulated mainly in the deep soil layers (Glomus magnicaule in Allenrolfea patagonica, Septoglomus aff. constrictum in Atriplex argentina), others mainly in the top layers (G. brohultti in Atriplex argentina and Septoglomus aff. constrictum in Allenrolfea patagonica). Although the low percentages of colonization or lack of it, our results show a moderate diversity of AMF associated to the species of Chenopodiaceae investigated in this study. The taxonomical diversity reveals that AMF are adapted to extreme environmental conditions from saline soils of central Argentina.